Challenges from Soil Variability, Johan Castberg Field, Barents Sea

C. Forsberg, E. Solhjell, V. Karlsen, V. Vangen
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Abstract

As development concepts for the Johan Castberg Field matured, new locations required soil data. A harder layer has been identified from previous soil data and mapped on seismic profiles as Seismic Unit II. This layer may cause refusal of suction anchor penetration and should ideally be avoided. Predictions of the depth to this layer both along and between seismic profiles were used to optimize suction anchor locations to be investigated during the 2018 soil investigation. This campaign was furthermore optimized by taking earlier laboratory testing into consideration. The Nkt factors were given special attention and found not to vary much in the topmost soil layers. Greater emphasis could therefore be put on acquiring CPTU data, and to use these previously determined Nkt factors to find the soil strength. The predictions of the depths to the top of Seismic Unit II were in general agreement with the data acquired during the 2018 investigation. The emphasis on collecting CPTU data and combining these with experience from the previous soil testing results saved both ship time and laboratory costs.
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巴伦支海Johan Castberg油田土壤变异性带来的挑战
随着Johan Castberg油田开发理念的成熟,新地点需要土壤数据。从以前的土壤数据中确定了一个较硬的层,并在地震剖面上绘制为地震单元II。这一层可能会导致吸力锚渗透的拒绝,最好避免。在2018年的土壤调查中,利用沿地震剖面和地震剖面之间的深度预测来优化将要调查的吸力锚点位置。考虑到早期的实验室测试,进一步优化了这一活动。对Nkt因子进行了特别的研究,发现Nkt因子在最上层土壤中变化不大。因此,更大的重点可以放在获取CPTU数据上,并使用这些先前确定的Nkt因子来找到土壤强度。第二地震单元顶部深度的预测与2018年调查期间获得的数据基本一致。重点是收集CPTU数据,并将这些数据与以前土壤测试结果的经验相结合,节省了船舶时间和实验室成本。
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